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《Mineral Deposits》 2012-01
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Fluid inclusion characteristics of typical uranium deposits in Xiangshan orefield,Jiangxi Province

ZHANG ShuMing1~4,CAO ShouSun1,4,Zeng WenLe4,RAO ZeHuang1,XIE GuoFa4,FANG Xin2,ZHANG Ying2,WANG Lei2 and ZHANG Xin3(1 Key Laboratory of Radioactive Geology and Exploration Technology Fundamental Science for National Defense,East China Institute of Technology,Fuzhou 344000,Jiangxi,China;2 State Key Laboratory Breeding Base of Nuclear Resources and Environment,East China Institute of Technology,Nanchang 330013,Jiangxi,China;3 Digital Land Key Laboratory of Jiangxi Province,East China Institute of Technology,Fuzhou 344000,Jiangxi,China;4 No.261 Geological Party,Jiangxi Bureau of Geology for Nuclear Industry,Yingtan 335001,Jiangxi,China)  
Based on a study of the fluid inclusions in fluorite from the Zoujianshan,Hengjian and Shazhou uranium deposits in the Xiangshan uranium orefield of Jiangxi,the authors have drawn the conclusions as follows: In the Zoujiashan uranium deposit,the average homogenization temperatures of fluid inclusions are 266.1℃ and 159.9℃ at the elevations of-130 m and 206 m,the average salinities w(NaCleq) are 11.61% and 13.16%,and the mean densities of fluorite inclusions are 0.88 g/cm3 and 1.00 g/cm3,suggesting that the regularity of homogenization temperature and salinity is of the parabola type;the density and homogenization temperature are significantly of negative correlation,and the density and salinity are of positive correlation.In the Hengjian uranium deposit,the average homogenization temperatures of fluid inclusions at the elevations of-3 m and 92 m are 259.9℃ and 291.7℃ respectively,the average salinities w(NaCleq) are 13.45% and 7.95%,and the mean densities are 0.91 g/cm3 and 0.79 g/cm3.The density and homogenization temperature are obviously of negative correlation,and the density and salinity do not show obvious correlation.In the Shazhou uranium deposit,the average homogenization temperatures of fluid inclusions are 297.3℃ and 272.9℃ at the elevations of-138 m and-98 m,the average salinities w(NaCleq) are 13.73% and 11.62%,and the mean densities of fluorite inclusions are 0.86 g/cm3 and 0.87 g/cm3,suggesting that the regularity of homogenization temperature and salinity is inconspicuous,the density and homogenization temperature are significantly of negative correlation,and the relationship between density and salinity is not obvious.In the Zoujiashan ore deposit,the average uranium metallogenic depths at the elevations of-130 m and 206 m are 860 m and 550 m,measured by the fluid inclusion method.In the Hengjian ore deposit,the average uranium metallogenic depths at the elevations of-3 m and 92 m are 930 m and 950 m.In the Shazhou ore deposit,the average uranium metallogenic depths at the elevations of-138 m and-98 m are 578 m and 537 m.A comparison with the surface elevation shows that the denudation depths after the formation of the Zoujiashan,Hengjian and Shazhou uranium deposits are respectively 320~416 m,190~240 m,and 727~902 m.The extent of uplift and erosion in northwestern Xiangshan is more serious than that in southeastern Xiangshan area,and the deep areas of eastern and southern Xiangshan have favorable ore-search prospect.
【Fund】: 国家自然科学基金项目(编号:41172079);; 江西省数字国土重点实验室开放基金(编号:DLLJ201104);; 江西省教育厅科研项目(编号:GJJ08307)的联合资助
【CateGory Index】: P619.14
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